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  • 1
    Schlagwort(e): basin research ; cratonic basin ; Parnaíba Basin ; Brazil
    Beschreibung / Inhaltsverzeichnis: Cratonic basin formation: a case study of the Parnaíba Basin of Brazil / M. C. Daly, R. A. Fuck, J. Julià, D. I. M. Macdonald and A. B. Watts / Geological Society, London, Special Publications, 472, 1-15, 14 September 2018, https://doi.org/10.1144/SP472.20 --- Cratonic basins --- Cratonic basins with reference to the Michigan basin / Norman H. Sleep / Geological Society, London, Special Publications, 472, 17-35, 6 February 2018, https://doi.org/10.1144/SP472.1 --- Lithospheric heating by crustal thickening: a possible origin of the Parnaíba Basin / D. McKenzie and V. Rodríguez Tribaldos / Geological Society, London, Special Publications, 472, 37-44, 19 February 2018, https://doi.org/10.1144/SP472.5 --- A comparative study of the Parnaíba, Michigan and Congo cratonic basins / A. B. Watts, B. Tozer, M. C. Daly and J. Smith / Geological Society, London, Special Publications, 472, 45-66, 22 February 2018, https://doi.org/10.1144/SP472.6 --- The Parnaíba cratonic basin: lithospheric and crustal structure --- Structure of the crust and upper mantle beneath the Parnaíba Basin, Brazil, from wide-angle reflection–refraction data / José E. P. Soares, Randell Stephenson, Reinhardt A. Fuck, Marcus V. A. G. de Lima, Vitto C. M. de Araújo, Flávio T. Lima, Fábio A. S. Rocha and Cíntia R. da Trindade / Geological Society, London, Special Publications, 472, 67-82, 13 April 2018, https://doi.org/10.1144/SP472.9 --- Deep crustal architecture of the Parnaíba basin of NE Brazil from receiver function analysis: implications for basin subsidence / Diogo L. O. Coelho, Jordi Julià, Verónica Rodríguez-Tribaldos and Nicholas White / Geological Society, London, Special Publications, 472, 83-100, 16 May 2018, https://doi.org/10.1144/SP472.8 --- Reprocessing and interpretation of deep structures in a regional transect of the Parnaíba Basin, Brazil / Rafael R. Manenti, Wilker E. Souza and Milton J. Porsani / Geological Society, London, Special Publications, 472, 101-107, 12 June 2018, https://doi.org/10.1144/SP472.17 --- Electrical conductivity structure across the Parnaíba Basin, NE Brazil / F. F. Solon, S. L. Fontes and E. F. La Terra / Geological Society, London, Special Publications, 472, 109-126, 13 July 2018, https://doi.org/10.1144/SP472.19 --- The pre-Silurian Riachão basin: a new perspective on the basement of the Parnaíba basin, NE Brazil / Amanda Porto, Michael C. Daly, Emanuele La Terra and Sergio Fontes / Geological Society, London, Special Publications, 472, 127-145, 19 February 2018, https://doi.org/10.1144/SP472.2 --- Implications of preliminary subsidence analyses for the Parnaíba cratonic basin / Verónica Rodríguez Tribaldos and Nicky White / Geological Society, London, Special Publications, 472, 147-156, 6 February 2018, https://doi.org/10.1144/SP472.3 --- The Parnaíba cratonic basin: stratigraphic and sedimentological evolution --- Evolution of a cratonic basin: insights from the stratal architecture and provenance history of the Parnaíba Basin / L. A. Menzies, A. Carter and David I. M. MacDonald / Geological Society, London, Special Publications, 472, 157-179, 6 August 2018, https://doi.org/10.1144/SP472.18 --- Provenance of sandstones in the Parnaíba Basin through detrital zircon geochronology / M. H. B. M. Hollanda, A. M. Góes and F. A. Negri / Geological Society, London, Special Publications, 472, 181-197, 12 July 2018, https://doi.org/10.1144/SP472.16 --- Palaeogeographical and palaeoclimatic evolution of the intracratonic Parnaíba Basin, NE Brazil using GPlates plate tectonic reconstructions and chemostratigraphic tools / Marwan M. Jaju, Haydon P. Mort, Fadi H. Nader, Mário L. Filho and David I. M. Macdonald / Geological Society, London, Special Publications, 472, 199-222, 6 June 2018, https://doi.org/10.1144/SP472.12 --- Re-evaluation of the Permian macrofossils from the Parnaíba Basin: biostratigraphic, palaeoenvironmental and palaeogeographical implications / Roberto Iannuzzi, Rodrigo Neregato, Juan C. Cisneros, Kenneth D. Angielczyk, Ronny Rößler, Rosemarie Rohn, Claudia Marsicano, Jörg Fröbisch, Thomas Fairchild, Roger M. H. Smith, Francine Kurzawe, Martha Richter, Max C. Langer, Tatiane M. V. Tavares, Christian F. Kammerer, Domingas M. Conceição, Jason D. Pardo and Guilherme A. Roesler / Geological Society, London, Special Publications, 472, 223-249, 2 July 2018, https://doi.org/10.1144/SP472.14 --- The Parnaíba cratonic basin: magmatic history --- Geochemical and temporal provinciality of the magmatism of the eastern Parnaíba Basin, NE Brazil / Monica Heilbron, Eliane Guedes, Miguel Mane, Claudio de Morisson Valeriano, Miguel Tupinambá, Júlio Almeida, Luiz Guilherme do Eirado Silva, Beatriz Paschoal Duarte, Jorge Carlos Dela Favera and Adriano Viana / Geological Society, London, Special Publications, 472, 251-278, 5 June 2018, https://doi.org/10.1144/SP472.11 --- Petrology of Jurassic and Cretaceous basaltic formations from the Parnaíba Basin, NE Brazil: correlations and associations with large igneous provinces / Alisson L. Oliveira, Márcio M. Pimentel, Reinhardt A. Fuck and Diógenes C. Oliveira / Geological Society, London, Special Publications, 472, 279-308, 6 August 2018, https://doi.org/10.1144/SP472.21 --- Role of basaltic magmatism within the Parnaíba cratonic basin, NE Brazil / Marthe Klöcking, Nicky White and John MacLennan / Geological Society, London, Special Publications, 472, 309-319, 23 March 2018, https://doi.org/10.1144/SP472.4 --- Phanerozoic magmatism in the Parnaíba Basin: characterization of igneous bodies (well logs and 2D seismic sections), geometry, distribution and sill emplacement patterns / I. Trosdtorf, J. M. Morais Neto, S. F. Santos, C. V. Portela Filho, T. A. Dall Oglio, A. C. M. Galves and A. M. Silva / Geological Society, London, Special Publications, 472, 321-340, 16 May 2018, https://doi.org/10.1144/SP472.10 --- The Parnaíba cratonic basin: resource system --- Atypical igneous-sedimentary petroleum systems of the Parnaíba Basin, Brazil: seismic, well logs and cores / Frederico S. de Miranda, Ana Luiza Vettorazzi, Paulo R. da Cruz Cunha, Fernando B. Aragão, Diogo Michelon, João Luiz Caldeira, Ernani Porsche, Celso Martins, Roberto B. Ribeiro, Alexandre F. Vilela, José R. Corrêa, Lilian S. Silveira and Kátia Andreola / Geological Society, London, Special Publications, 472, 341-360, 12 July 2018, https://doi.org/10.1144/SP472.15 --- New insights into the Parnaíba Basin: results of investments by the Brazilian National Petroleum Agency / Marina Abelha, Eliane Petersohn, Gabriel Bastos and Daniel Araújo / Geological Society, London, Special Publications, 472, 361-366, 5 July 2018, https://doi.org/10.1144/SP472.13
    Seiten: Online-Ressource (VIII, 372 Seiten) , Illustrationen, Diagramme
    ISBN: 9781786203960
    Sprache: Englisch
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2018-12-20
    Print ISSN: 0305-8719
    Digitale ISSN: 2041-4927
    Thema: Geologie und Paläontologie
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2018-01-01
    Print ISSN: 0305-8719
    Digitale ISSN: 2041-4927
    Thema: Geologie und Paläontologie
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
  • 5
    Publikationsdatum: 2015-03-09
    Beschreibung: The North Sakhalin Basin in the western Sea of Okhotsk has been the main site of sedimentation from the Amur River since the Early Miocene. In this article, we present regional seismic reflection data and a Neogene-Recent sediment budget to constrain the evolution of the basin and its sedimentary fill, and consider the implications for sediment flux from the Amur River, in particular testing models of continental-scale Neogene drainage capture. The Amur-derived basin-fill history can be divided into five distinct stages: the first Amur-derived sediments (〉21-16.5 Ma) were deposited during a period of transtension along the Sakhalin-Hokkaido Shear Zone, with moderately high sediment flux to the basin (71 Mt year-1). The second stage sequence (16.5-10.4 Ma) was deposited following the cessation of transtension, and was characterised by a significant reduction in sediment flux (24 Mt year-1) and widespread retrogradation of deltaic sediments. The third (10.4-5.3 Ma) and fourth (5.3-2.5 Ma) stages were characterised by progradation of deltaic sediments and an associated increase in sediment flux (48-60 Mt year-1) to the basin. Significant uplift associated with regional transpression started during this time in southeastern Sakhalin, but the north-eastward propagating strain did not reach the NE shelf of Sakhalin until the Pleistocene (〈2.5 Ma). This uplift event, still ongoing today, resulted in recycling of older deltaic sediments from the island of Sakhalin, and contributed to a substantially increased total sediment flux to the adjacent basinal areas (165 Mt year-1). Adjusted rates to discount these local erosional products (117 Mt year-1) imply an Amur catchment-wide increase in denudation rates during the Late Pliocene-Pleistocene however, this was likely a result of global climatic and eustatic effects, combined with tectonic processes within the Amur catchment and possibly a smaller drainage capture event by the Sungari tributary, rather than continental-scale drainage capture involving the entire upper Amur catchment. © 2016 John Wiley & Sons Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists.
    Print ISSN: 0950-091X
    Digitale ISSN: 1365-2117
    Thema: Geologie und Paläontologie
    Publiziert von Wiley
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2020-04-17
    Beschreibung: The North Sakhalin Basin in the western Sea of Okhotsk has been the main site of sedimentation from the Amur River since the Early Miocene. In this article, we present regional seismic reflection data and a Neogene–Recent sediment budget to constrain the evolution of the basin and its sedimentary fill, and consider the implications for sediment flux from the Amur River, in particular testing models of continental‐scale Neogene drainage capture. The Amur‐derived basin‐fill history can be divided into five distinct stages: the first Amur‐derived sediments (〉21–16.5 Ma) were deposited during a period of transtension along the Sakhalin‐Hokkaido Shear Zone, with moderately high sediment flux to the basin (71 Mt year−1). The second stage sequence (16.5–10.4 Ma) was deposited following the cessation of transtension, and was characterised by a significant reduction in sediment flux (24 Mt year−1) and widespread retrogradation of deltaic sediments. The third (10.4–5.3 Ma) and fourth (5.3–2.5 Ma) stages were characterised by progradation of deltaic sediments and an associated increase in sediment flux (48–60 Mt year−1) to the basin. Significant uplift associated with regional transpression started during this time in southeastern Sakhalin, but the north‐eastward propagating strain did not reach the NE shelf of Sakhalin until the Pleistocene (〈2.5 Ma). This uplift event, still ongoing today, resulted in recycling of older deltaic sediments from the island of Sakhalin, and contributed to a substantially increased total sediment flux to the adjacent basinal areas (165 Mt year−1). Adjusted rates to discount these local erosional products (117 Mt year−1) imply an Amur catchment‐wide increase in denudation rates during the Late Pliocene–Pleistocene; however, this was likely a result of global climatic and eustatic effects, combined with tectonic processes within the Amur catchment and possibly a smaller drainage capture event by the Sungari tributary, rather than continental‐scale drainage capture involving the entire upper Amur catchment.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Erwartet Verfügbarkeit
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